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Mount Adatara

Adatarayama

Stratovulcano · Japan · 1728 m

The broad Adatara massif is composed of a group of cones and lava domes, seen here from the W. The unvegetated area on the left summit ridge is a 1-km-wide circular crater that has been mined for sulfur. Seventy-two miners working in the crater were killed during an explosive eruption in 1900.
The broad Adatara massif is composed of a group of cones and lava domes, seen here from the W. The unvegetated area on the left summit ridge is a 1-km-wide circular crater that has been mined for sulfur. Seventy-two miners working in the crater were killed during an explosive eruption in 1900. · Foto: Photo by Lee Siebert, 1988 (Smithsonian Institution). · Wikimedia Commons
Tipo
Stratovulcano
Paese
Japan
Regione
Northwestern Pacific Volcanic Regions / Northeast Japan Volcanic Arc
Altitudine
1728 m
Coordinate
37.647, 140.281
Ultima eruzione
1996
Contesto tettonico
Subduction zone / Continental crust (> 25 km)
Forma vulcanica
Composite
Roccia principale
Andesite / Basaltic Andesite
Sintesi geologica

The broad forested massif of Adatarayama volcano is located E of Bandai volcano, about 15 km SW of Fukushima city. It consists of a group of dominantly andesitic stratovolcanoes and lava domes that rise above Tertiary rocks on the south and abut Azumayama volcano on the north. Construction took place in three main stages that began about 550,000, 350,000, and 200,000 years ago. The high point of the complex is 1728-m-high Minowasan, a dome-shaped stratovolcano north of Tetsuzan, the currently active stratovolcano. Numanotaira, the active summit crater, is surrounded by hot springs and fumaroles and is breached by the Iogawa river ("Sulfur River") on the west. Seventy-two workers of a sulfur mine in the summit crater were killed during an eruption in 1900. Historical eruptions have been restricted to the 1.2-km-wide, 350-m-deep Numonotaira crater.

Sintesi da Wikipedia

Riassunto in inglese

Riassunto breve — apri l'articolo completo per maggiori dettagli.

Mount Adatara is a stratovolcano in Fukushima Prefecture, Japan.

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Storia delle eruzioni

Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni
8050 BCE~7715 BCE · 1 eruzioni · VEI max. 36711 BCE~6376 BCE · 1 eruzioni · VEI max. 36376 BCE~6041 BCE · 1 eruzioni · VEI max. 34366 BCE~4032 BCE · 1 eruzioni · VEI max. 32692 BCE~2357 BCE · 1 eruzioni · VEI max. 31688 BCE~1353 BCE · 1 eruzioni · VEI max. ?683 BCE~348 BCE · 1 eruzioni · VEI max. 3348 BCE~13 BCE · 1 eruzioni · VEI max. ?657~991 · 1 eruzioni · VEI max. ?1661~1996 · 4 eruzioni · VEI max. 28050 BCE5706 BCE3027 BCE683 BCE1661

Cronologia dettagliata

  1. 1996VEI 1Osservata
    1996-09-01 – 1996-09-01
    Numanotaira
  2. 1900VEI 2Osservata
    1900-07-17 – 1900-07-17
    Numanotaira
  3. 1899VEI 2Osservata
    1899-08-24 – 1899-11-12
    Numanotaira
  4. 1813VEI 1Stima geologica
    1813-01-10 – In corso
    Numanotaira
  5. 950 (±50 anni)VEI ?Stima geologica
    950 – In corso
    Numanotaira
  6. 50 a.C. (±900 anni)VEI ?Stima geologica
    BCE 50 – In corso
    Numanotaira
  7. 590 a.C. (±200 anni)VEI 3Stima geologica
    BCE 590 – In corso
    Numanotaira
  8. 1550 a.C. (±1100 anni)VEI ?Stima geologica
    BCE 1550 – In corso
    Numanotaira
  9. 2600 a.C. (±50 anni)VEI 3Stima geologica
    BCE 2600 – In corso
    Numanotaira
  10. 4300 a.C. (±850 anni)VEI 3Stima geologica
    BCE 4300 – In corso
    Numanotaira
  11. 6150 a.C. (±100 anni)VEI 3Stima geologica
    BCE 6150 – In corso
    Numanotaira
  12. 6650 a.C. (±100 anni)VEI 3Stima geologica
    BCE 6650 – In corso
    Numanotaira
  13. 8050 a.C.VEI 3Stima geologica
    BCE 8050 – In corso
    Numanotaira

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